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Bamfordite

A valid IMA mineral species
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About BamforditeHide

Formula:
Fe3+Mo2O6(OH)3 · H2O
Colour:
Apple-green
Lustre:
Vitreous, Earthy
Hardness:
2 - 3
Specific Gravity:
3.620
Crystal System:
Triclinic
Name:
After its locality.
This page provides mineralogical data about Bamfordite.


Unique IdentifiersHide

Mindat ID:
6815
Long-form identifier:
mindat:1:1:6815:0

IMA Classification of BamforditeHide

Classification of BamforditeHide

4.FK.05

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
F : Hydroxides (without V or U)
K : Hydroxides with H2O +- (OH); chains of edge-sharing octahedra

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

SymbolSourceReference for Standard
BfdIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of BamforditeHide

Vitreous, Earthy
Transparency:
Transparent
Colour:
Apple-green
Streak:
Greenish yellow
Hardness:
2 - 3 on Mohs scale
Cleavage:
Distinct/Good
(100)
Comment:
Compact to friable in aggregates
Density:
3.620(8) g/cm3 (Measured)    3.616 g/cm3 (Calculated)

Optical Data of BamforditeHide

Type:
Biaxial (-)
RI values:
nα = 1.91(1) nβ = 2.03(1) nγ = 2.11(1)
2V:
Measured: 90° , Calculated: 74°
Max. Birefringence:
δ = 0.200
Based on recorded range of RI values above.

Interference Colours:
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.

Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.

Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.

Surface Relief:
Very High (positive)
Relative to Canada balsam mounting medium (n ≈ 1.537).

This shows the grain boundary and Becke line effect under plane-polarised light, based on the contrast between this mineral's average refractive index and the mounting medium. It does not take into account mineral colouration.
In focus
Interference Figure:
This shows the idealized biaxial acute bisectrix (Bxa) interference figure - the conoscopic view for a grain cut perpendicular to the acute bisectrix, using this mineral's 2V. The two small white dots mark the melatopes - the points where the two optic axes emerge - and are shown only when they fall within the field of view. The coloured bands are isochromatics, and the dark bands are isogyres.

Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Dispersion:
r < v
Pleochroism:
Weak
Comments:
Pale to moderate; in yellowish greens

Chemistry of BamforditeHide

Mindat Formula:
Fe3+Mo2O6(OH)3 · H2O
Element Weights:
Element% weight
Mo46.492 %
O38.758 %
Fe13.528 %
H1.221 %

Calculated from ideal end-member formula.
Mo
O
Fe
H

Crystallography of BamforditeHide

Crystal System:
Triclinic
Class (H-M):
1 - Pinacoidal
Space Group:
P1
Cell Parameters:
a = 5.889(5) Å, b = 7.545(5) Å, c = 9.419(5) Å
α = 71.46(4)°, β = 83.42(4)°, γ = 72.78(4)°
Ratio:
a:b:c = 0.781 : 1 : 1.248
Unit Cell V:
378.91 ų (Calculated from Unit Cell)
Z:
2

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0001962BamforditeBirch W D, Pring A, McBriar E M, Gatehouse B M, McCammon C A (1998) Bamfordite, a new hydrated iron molybdenum oxyhydroxide from Queensland, Australia: Description and crystal chemistry American Mineralogist 83 172-17719980293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
47a : [Near-surface hydration of prior minerals]

Type Occurrence of BamforditeHide

General Appearance of Type Material:
Apple green with yellowish tint
Place of Conservation of Type Material:
South Australian Museum, Adelaide, 20653; Museum of Victoria, Melbourne, Australia, M7424.
Geological Setting of Type Material:
Oxidation zone of greisen
Associated Minerals at Type Locality:

Synonyms of BamforditeHide

Other Language Names for BamforditeHide

Other InformationHide

Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.

Internet Links for BamforditeHide

References for BamforditeHide

Localities for BamforditeHide

Showing 1 localities.

This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The symbol next to localities in the list can be used to jump to that position on the map.
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Locality ListHide

- This locality has map coordinates listed. - This locality has estimated coordinates. ⓘ - Click for references and further information on this occurrence. ? - Indicates mineral may be doubtful at this locality. - Good crystals or important locality for species. - World class for species or very significant. (TL) - Type Locality for a valid mineral species. (FRL) - First Recorded Locality for everything else (eg varieties). Struck out - Mineral was erroneously reported from this locality. Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).

All localities listed without proper references should be considered as questionable.
Australia (TL)
 
  • Queensland
    • Mareeba Shire
      • Bamford
Birch et al. (1998)
 
and/or  
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